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”ŽŽm

•½¬25”N3ŒŽC—¹(•½¬24”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
¬¼ Œ’‰îWaveform inversion for localized 3-D seismic velocity structure in the lowermost mantle beneath the Western Pacific
íî“c —m•½Investigation of slip parameters and fault slip behavior in the shallow part of subduction zone on the basis of vitrinite reflectance

•½¬22”N3ŒŽC—¹(•½¬21”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
ã–Ø Œ«‘¾Origin of arc magmas in the Sengan region, Northeastern Japan and Thermodynamic modeling of mantle melting
•yŽm ‰„ÍA methodology for inversion of seismic waveforms for elastic and anelastic structure and its preliminary application to the mantle transition zone benath the Northwestern Pacific

•½¬21”N3ŒŽC—¹(•½¬20”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
Tae-Ho PARKChronological and Petrological Study of Cretaceous to Paleogene Granitic Rocks, South Korea
‰ª“c ^‰îCrustal extension and shortening in the back-arc region of Northeast Japan
òŽR “O–çIncremental melting process and thermal evolution of an upwelling mantle: constraints from back arc volcanisms in the eastern margin of the Eurasian Plate
“ào ’•FObservational study on the self-similarity of earthquake rupture growth in Parkfield area
²“¡ —FŽqSiO2 ƒKƒ‰ƒX‚Ì–§“x‚ƍ\‘¢‚Ì’´‚ˆ³‰º‚»‚̏ꑪ’è
–ì“c Žé”üGPS Data Inversion to Estimate 3-D Elastic/Inelastic Strain Fields in Island-Arc Crust
ŽRŒû ”ò’¹Linkage between faulting, fluid flow and earthquake generation in seismogenic subduction zones

•½¬20”N9ŒŽC—¹(•½¬20”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
Ž­‘q —m‰îNumerical Simulation with a Finite Element Method for the Development of Mechanical and Thermal Structure in Subduction Zones

•½¬20”N3ŒŽC—¹(•½¬19”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
‰¬’à ’BWater content of the upper mantle benearth island arcs and its tectonic implications: Petrologic study of Aogashima Volcano, Izu Arc, Japan
—é–Ø ÊŽqNew deformation indicator for peridotites in the upper mantle: Experimental study on diffusion in chromite spinel
ì’[ ŒP‘ãQuantitative examinations of mass transfer by pressure solution and fluid flow in natural deformation zones

•½¬19”N3ŒŽC—¹(•½¬18”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
•½—Ñ LNDevelopment of a finite-difference scheme using optimally accurate operators for computation of synthetic seismograms in heterogeneous media and its applicability to geophysical exploration

•½¬18”N9ŒŽC—¹(•½¬18”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
‹´ŠÔ º“¿Internal Deformation Fields due to a Moment Tensor in an Elastic-Viscoelastic Layered Half-Space: Application to Tectonics of Back-Arc Basins
–k‘º —LvA fate of sediments in subduction zone
’†‘º m”üGeochemical variations of volcanic rocks in Central Japan: Implication for the fluid processes in subduction zone with the double subducting plates

•½¬18”N3ŒŽC—¹(•½¬17”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
Ž›ì ŽõŽqAbsolute Strength of the San Andreas Fault Inferred from Tectonic Loading Simulation and CMT Data Inversion
‰Í‡ Œ¤ŽuMethods for waveform inversion for localized seismic structure

•½¬16”N3ŒŽC—¹(•½¬15”N“x)

Ž–¼˜_•¶‘è–Ú—vŽ|
“c—Í ³D‘æŽl‹IŒãŠú‚É‚¨‚¯‚é“Œ–k“ú–{ŒÊ‚Ì’nŠk•Ï“®pdf
Žu‘º —æŽq”óƒ}ƒOƒ}—­‚Ü‚è‚Ì”M‰»Šwi‰»‰ß’öF”[¹•z–¦ŠÑ“üŠâ‘Ì‚©‚ç‚̐§–ñpdf

CŽm

•½¬25”N3ŒŽC—¹i•½¬24”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
ŒÜ\—’ ŒõŽk‹‘å’nk‚ÌŽ©—RU“®‚ð—p‚¢‚½‚ä‚Á‚­‚è‚Æ‚µ‚½‚·‚ׂè‚ÌŒŸoƒQƒ‰[ ƒƒo[ƒg

•½¬24”N3ŒŽC—¹i•½¬23”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
ŒIŒ´ ‹`Ž¡Statistical analysis of seismicity by discretized triggering model i—£ŽU“IƒgƒŠƒKƒŠƒ“ƒOƒ‚ƒfƒ‹‚É‚æ‚é’nkŠˆ“®‚Ì“Œv“I‰ðÍjˆäo “N
‰––¡ —I–çÆ«/‘Y«‘JˆÚ—̈æ‚É‚¨‚¯‚é™’’f‘Ñ‚Ì”ñ‘Ώ̐«‚ɂ‚¢‚Ă̍lŽ@“c’† GŽÀ
¼ŽR Œ’ŽuAnalysis of Size, Geometry, and Motion of PlatesiƒvƒŒ[ƒg‚̃TƒCƒYAŒ`A‰^“®‚̉ðÍj–Ø‘º Šw
–ƒ¶ ®•¶Intraplate Deep Low Frequency Earthquakes far from Active Volcanoes iŠˆ‰ÎŽR‚©‚ç—£‚ꂽƒvƒŒ[ƒg“à‚̐[•”’áŽü”g’nkjˆäo “N
‚“c Œ[l’á–§“xSiO2 Œ‹»‚̃wƒŠƒEƒ€’†‚ł̈³k‹““®‘DŽç “W³
’·’Jì ŒcSeismic Waveform Evidence for Existence of an Ultra-low Velocity Zone with Significant Amounts of Iron in the lowermost mantle beneath the central Pacific (’nk”gŒ`•ªÍ‚©‚玦´‚³‚ê‚é’†‰›‘¾•½—m‰ºƒ}ƒ“ƒgƒ‹Å‰º•”‚É‚¨‚¯‚é’´’ᑬ“x—̈æ‚Ì‘¶Ý)ƒQƒ‰[ ƒƒo[ƒg
”ä–¼ ËŽqDehydration and deformation processes of siliceous sediments in subduction zonesi’¾‚ݍž‚Ý‘Ñ‚É‚¨‚¯‚éŒ]Ž¿‘͐ϕ¨‚Ì’E…E•ÏŒ`‰ß’öj–Ø‘º Šw
Žá—Ñ ‘å—C‚–§“x‰»SiO2 ƒKƒ‰ƒX‚̈³k‹““®‘DŽç “W³

•½¬23”N3ŒŽC—¹i•½¬22”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
”Ñ“c ˜a–çChronology, Petrology and Numerical Simulation for Cretaceous to Paleogene Granitic Rocks, SW Japan i¼“ì“ú–{”’ˆŸ‹I]ŒÃ‘æŽO‹I‰Ô›¼Šâ—Þ‚Ì”N‘ãŠw“IEŠâÎŠw“IŒ¤‹†‚¨‚æ‚ѐ”’lŒvŽZjŠâX Œõ
”’à_ ‹g‹NALOS ‰æ‘œ‚ð—p‚¢‚½Kumukol Basin ‚Ì•Ï“®’nŒ`‰ðÍ‚ƃ`ƒxƒbƒg‚Œ´–k‰‚ÌŠg‘僁ƒJƒjƒYƒ€‚ÌŒŸ“¢’r“c ˆÀ—²

•½¬22”N3ŒŽC—¹i•½¬21”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
“c‘º T‘¾˜NEffects of Material Heterogeneity on Branching Faults in a Subduction System i’¾‚ݍž‚Ý‘Ñ‚Ì•ªŠò’f‘w‚ɑ΂·‚é”}Ž¿•s‹ÏŽ¿‚̉e‹¿jˆäo “N

•½¬21”N3ŒŽC—¹i•½¬20”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
‘¾“c ˜aWPrecise hypocenter distribution of deep low-frequency earthquakes and its relationship to the local geometry of the subducting plate in Nankai subduction zone, Japan (“ìŠCƒgƒ‰ƒt’¾‚ݍž‚Ý‘Ñ‚É‚¨‚¯‚é[•”’áŽü”g’nk‚̐¸–§kŒ¹•ª•z‚ƋǏŠ“I‚ȃvƒŒ[ƒg\‘¢‚Æ‚ÌŠÖŒW)ˆäo “N
“í“c ç•äGeochemical and numerical studies on slab-derived fluids and the Arima-type brine (ƒXƒ‰ƒu‹NŒ¹—¬‘Ì‚Æ—L”nŒ^‰–…‚ÉŠÖ‚·‚é’n‹…‰»Šw ‚¨‚æ‚ѐ”’lƒ‚ƒfƒŠƒ“ƒOŒ¤‹†)ŠâX Œõ
¬¼ Œ’‰îShear velocity structure in the lowermost mantle beneath the western Pacific from waveform inversion i”gŒ`ƒCƒ“ƒo[ƒWƒ‡ƒ“‚É‚æ‚鐼‘¾•½—m‰º‚̍ʼnº•”ƒ}ƒ“ƒg ƒ‹S ”g‘¬“x\‘¢„’èjƒQƒ‰[ ƒƒo[ƒg
¬—Ñ ¡“úŽqDiagenesis, dehydration and deformation of pelagic sediments in ancient subduction zone inferred from bedded chert in the Inuyama area, Mino Belt i’¾‚Ý ž‚Ý‘Ñ‚É‚¨‚¯‚éƒ`ƒƒ[ƒg‘w‚Ì‘±¬E’E…‚Æ•ÏŒ`‚ÌŠÖŒW-”ü”Z‘ÑŒ¢ŽR’nˆæ‚æ‚è-j–Ø‘º Šw
–ì’à ‘¾ˆêParticle Analysis and Energetics of Fault Rocks: An Example from the Toyamagawa Fault, Central Japan i’·–쌧‰“ŽRì’f‘w‚ð—á‚Æ‚µ‚½C’f‘wŠâ‚Ì—±Žq‰ðÍ‹y‚уGƒlƒ‹ƒM[˜_j“c’† GŽÀ

•½¬20”N3ŒŽC—¹i•½¬19”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
‰iˆä GŒ›Experimental Study of Pressure Effects on Microstructure of Partially-Molten Forsterite-Jadeite System i•”•ª—n—ZƒtƒHƒ‹ƒXƒeƒ‰ƒCƒg[ƒqƒXƒC‹PÎŒn‚Ì”÷×\‘¢‚ւ̈³—ÍŒø‰Ê‚ÌŽÀŒ±“IŒ¤‹†j¬àV ˆêm
ãžŠ —T‹v’PŽÎ‹PÎƒ|[ƒtƒBƒƒNƒ‰ƒXƒg‚ð—p‚¢‚½ƒ}ƒ“ƒgƒ‹‚©‚ñ‚ç‚ñŠâ‚̉·“x-ˆ³—Í-•ÏŒ`Žw•W `–y–ž‚©‚ñ‚ç‚ñŠâ‘̂̏㏸—š—ð‚Ö‚Ì“K‰ž¬àV ˆêm
‘—t —zŽqShear zone growth on the splay fault in accretionary prism |the footwall of the Nobeoka Thrust in the Shimanto Belt (‹ãBŽl–œ\‘щ„‰ªÕã’f‘w‚©‚猩‚éout-of-sequence- thrust‚Ì™’’f‘Ñ‚Ì”­’B)–Ø‘º Šw
œAì ’q—²Õ’Ðì’f‘w‚É‚¨‚¯‚é, ”÷¬’nk‘½”­/‹ó”’—̈æ‚Ì’f‘wŠâ”äŠrŒ¤‹†“c’† GŽÀ
–kžŠ ˆ¤Deformation and diagenesis of sandstones in underthrusted sediments -An example from the Mugi Melange, Shikoku, Japan- i•t‰Á‘Ì’†‚̑͐ϕ¨‚ªŽó‚¯‚鑱¬‚¨‚æ‚Ñ•ÏŒ`‰ß’ö-Žl–œ\‘Ñ–´Šòƒƒ‰ƒ“ƒWƒ…‚Ì—á-j–Ø‘º Šw
¼”ö r•Fƒ_ƒCƒ„ƒ‚ƒ“ƒhƒAƒ“ƒrƒ‹‘•’u—pc-BNƒKƒXƒPƒbƒgŠJ”­‚Æ‚»‚̉ž—p‘DŽç “W³

•½¬19”N3ŒŽC—¹i•½¬18”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
²X–Ø •Ï¬Šâ’†‚ÉŒ»‚ê‚éå÷‹È\‘¢‚ÌŒ`¬‰ß’öŠâX Œõ
‰ª–{ L–çSlip mechanisms of a major out-of-sequence thrust in an accretionary complex ]Approaching from the Nobeoka Thrust in the Shimanto Belt, Kyushu Japan]–Ø‘º Šw
ꎓ¡ —F”äŒÃÕ’Ðì’f‘w”jÓ‘Ñ‚Ì’f‘wŠâƒRƒA‚ð—p‚¢‚½’nŠkƒKƒX¶¬^•úoŽÀŒ±“c’† GŽÀ
‚‹´ ˆŸ—[Young lava field on the old Pacific Plate just before its subduction: Volcanism induced by lithospheric flexureŠâX Œõ
•Ÿ‘º GŽ¡A model combining the Earth's thermal evolution and material fractionationŠâX Œõ
•yŽm ‰„Í1-D SH velocity models for the subregions of the Northwestern Pacific obtained using waveform inversionƒQƒ‰[ ƒƒo[ƒg

•½¬18”N3ŒŽC—¹i•½¬17”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
ã–Ø Œ«‘¾Subduction zone magmatism and mantle wedge structure of the Sengan region, Northeastern JapanŠâX Œõ
“ào ’•FDevelopment of Multiscale Slip Inversion Method and Its Application to the 2004 Mid-Niigata Prefecture Earthquakeˆäo “N
‰Y“c ‹IŽqƒ_ƒCƒŒ[ƒ^ƒ“ƒV[‚ðl—¶‚µ‚½thermal pressurization ƒ‚ƒfƒ‹‚Ì’nk’f‘w‚Ö‚Ì“K—p-–쓇’f‘wAŽÔâĚ¼’f‘w‚ð—á‚É‚µ‚Ä-“c’† GŽÀ
¬“c WˆÉ“ß’J’f‘w‘т̍\‘¢‚Æ‚»‚Ì”­’B‰ß’ö’r“c ˆÀ—²
¬“c“‡ —f_Cr-Al spinel as a deformation indicator for the upper mantle: observational study in the Horoman Peridotite Complex¬àV ˆêm
²“¡ —FŽq’´‚ˆ³‰º‚É‚¨‚¯‚é“ñŽ_‰»•¨‚Ìpost-PbCl2 ‘Š“]ˆÚ‚ÌŒ¤‹†‘DŽç “W³
–ì“c Žé”üInversion Analysis of Geodetic Data in the Kanto Region, Central Japan, with a 3-D Plate Interface Model: Diversity of Stress Release Modes¼‰Y [G
ŽRŒû ”ò’¹The origin of syntectonic veins in accretionary complex and its implication for fluid behavior around the up-dip limit of seismogenic zone–Ø‘º Šw

•½¬17”N3ŒŽC—¹i•½¬16”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
‰ª“c ^‰îƒXƒ“ƒ_ŠCa—¤‘¤ŽÎ–Ê‚ÌŠC’ê•Ï“®’nŒ`‚Æ‚»‚Ì”­’B‰ß’ö’r“c ˆÀ—²
òŽR “O–ç"Mechanism of mantle upwelling and melting in
back arc region: constraints from the temporal and spatial variation of the 'plateau basalt' in northwestern Kyushu"
¬àV ˆêm
–x“à r‰î"Numerical study of melting in subduction zones
with variable viscosity"
ŠâX Œõ

•½¬16”N3ŒŽC—¹i•½¬15”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
‘å•£ ’qŸƒvƒŒ[ƒg‹«ŠE‚É‚¨‚¯‚é’nk”­¶—lŽ®‚Ì‘½—l«‚ÉŠÖ‚·‚錤‹†¼‰Y [G
²“¡ ŠˆŽuA normal-faulting paleostress around the up-dip limit of seismogenic zone: An improvement of stress inversion method and its application to an onland accretionary complex–Ø‘º Šw
‹ß“¡ ‰pŽ÷Deformation and fluid flow through micro-cracks recorded in the Nobeoka thrust in the Shimanto Belt, Kyushu, Japan–Ø‘º Šw
Ž­‘q —m‰îNumerical Simulation for Geomorphic Evolution in Taiwan with a Stream Erosion Model¼‰Y [G

•½¬15”N3ŒŽC—¹i•½¬14”N“xj

Ž–¼˜_•¶‘è–ÚŽw“±‹³Š¯
‰¬’à ’BMechanisms of crustal differentiation of basaltic magmas: Constraints from the contrasting variation trends observed in Aogashima and@other Izu Arc volcanoes Œº•ŠâŽ¿ƒ}ƒOƒ}‚Ì’nŠk“à•ª‰»ƒƒJƒjƒYƒ€FÂƒ–“‡‚¨‚æ‚шɓ¤ŒÊ‰ÎŽR‚É‚Ý‚ç‚ê‚é‘ΏƓI‚ȕω»ƒgƒŒƒ“ƒh‚©‚ç‚̐§–ñ¬àV ˆêm
‰Í‡ Œ¤ŽuThe Direct Solution Method for computing synthetic seismograms in transversely isotropic spherically symmetric media and its applicationsƒQƒ‰[ ƒƒo[ƒg
ì’[ ŒP‘ãApllication of the isocon method to argillaceous rocks of accretionary complex and@quantitavive estimation of volume change due to mass transfer associated with deformation i•t‰Á‘Ì“DŽ¿Šâ‚Ö‚Ìisocon–@‚Ì“K—p‚Æ•ÏŒ`‚É”º‚¤Ž¿—ʈړ®‚É‚æ‚é‘̐ϕω»‚Ì’è—Ê“IŒ©Ï‚à‚èj–Ø‘º Šw
–k‘º —LvMagnetic fabric of underplated melange and its relationship with lithology of the@Shimanto Belt, southwest Japan i¼“ì“ú–{AŽl–œ\‘Ñ‚ÉŒ©‚é’ꂯƒƒ‰ƒ“ƒWƒ…‚ÌŽ¥«ƒtƒ@ƒuƒŠƒbƒN‚ÆŠâ‘Š‚Æ‚ÌŠÖŒWj–Ø‘º Šw
Ž›ì ŽõŽqƒTƒ“ƒAƒ“ƒhƒŒƒAƒXŒ^‰¡‚¸‚êƒvƒŒ[ƒg‹«ŠE‚̐â‘΋­“x„’菼‰Y [G
’†‘º m”ü—¼”’ŽR’n‚É‚¨‚¯‚é’¾‚ݍž‚ݑщΐ¬Šˆ“®ŠâX Œõ
•Ÿˆä Œ’ŽjDevelopment of a 3D Standard Model of Plate Interfaces in and around Japan: Physical Interpretation of Long-term Crustal@Movements in Kanto District i“ú–{—ñ“‡ˆæ‚ÌŽOŽŸŒ³ƒvƒŒ[ƒg‹«ŠEŒ`óƒ‚ƒfƒ‹‚̍\’zFŠÖ“Œ’nˆæ‚Ì’·Šú“I’nŠk•ÏŒ`‰^ “®‚̉𖾁j¼‰Y [G
¼‘º ³”VP-T condition and heterogeneous fluid flow through cracks in the underthrusted melange- observation from the Shimanto Belt, Japan i’¾‚ݍž‚ñ‚¾ƒƒ‰ƒ“ƒWƒ…‚É‚¨‚¯‚銄‚ê–Ú‚ð’Ê‚µ‚½•s‹ÏŽ¿‚È—¬‘Ì‚Ì—¬‚ê‚Ɖ·“xEˆ³—ÍðŒ[Žl–œ\‘Ñ ‚Å‚ÌŠÏŽ@j–Ø‘º Šw
ŽR–{ Žu”TXü‰ñÜ–@‚É‚æ‚éMgSiO3ƒƒ‹ƒg‚ÆCaSiO3ƒƒ‹ƒg‚̍\‘¢‚̈³—͕ω»‚ÌŒ¤‹†‘DŽç “W³
DJURAEV OmonEfficient and accurate methods for evaluating analytic solutions of the elastic equation of motion and their application to data analysis i‚¸“x‹y‚э‚ŒvŽZ”\—¦‚ð—L‚·‚é’e«‘̂̉^“®•û’öŽ®‚̉ðÍ“I‰ð‚«•û‚Æ‚»‚̉ž—pjƒQƒ‰[ ƒƒo[ƒg

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